Search results for "Geophysical monitoring"

showing 3 items of 3 documents

The 15 March 2007 explosive crisis at Stromboli Volcano, Italy: assessing physical parameters through a multidisciplinary approach

2011

Basaltic volcanoes are dominated by lava emission and mild explosive activity. Nevertheless, many basaltic systems exhibit, from time to time, poorly documented and little-understood violent explosions. A short-lived, multiblast explosive crisis (paroxysmal explosion) occurred on 15 March 2007 during an effusive eruptive crisis at Stromboli (Italy). The explosive crisis, which started at 20:38:14 UT, had a total duration of ∼5 min. The combined use of multiparametric data collected by the permanent instrumental networks (seismic, acoustic, and thermal records) and a field survey carried out immediately after the event enabled us to constrain the eruptive dynamics and quantify physical param…

DYNAMICSAtmospheric ScienceExplosive materialLavaPyroclastic flowSoil SciencePyroclastic rockAquatic ScienceOceanographyGeophysical monitoringEffusive eruptionImpact craterDEFORMATIONGeochemistry and Petrologyddc:550SR ISOTOPE EVIDENCE; EFFUSIVE ERUPTION; PAROXYSMAL EXPLOSION; PLUMBING SYSTEM; DYNAMICS; DEFORMATION; INSIGHTS; EVENT; TIME; CRYSTALLIZATIONEarth and Planetary Sciences (miscellaneous)StromboliParoxysmTephraEarth-Surface ProcessesWater Science and TechnologySR ISOTOPE EVIDENCEgeographygeography.geographical_feature_categoryEcologyTephra depositPLUMBING SYSTEMEFFUSIVE ERUPTIONPaleontologyForestryBallistic ejectionPAROXYSMAL EXPLOSIONVOLCANOLOGY INFRASOUND FALL-OUTTIMEINSIGHTSGeophysicsEVENTVolcanoSpace and Planetary ScienceCRYSTALLIZATIONScoriaGeologySeismology
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Internal dynamics and eruptive behaviour of Stromboli volcano

2015

Stromboli; Geophysical monitoringStromboliGeophysical monitoring
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Tracking dynamics of magma migration in open-conduit systems

2016

Open-conduit volcanic systems are typically characterized by unsealed volcanic conduits feeding permanent or quasi-permanent volcanic activity. This persistent activity limits our ability to read changes in the monitored parameters, making the assessment of possible eruptive crises more difficult. We show how an integrated approach to monitoring can solve this problem, opening a new way to data interpretation. The increasing rate of explosive transients, tremor amplitude, thermal emissions of ejected tephra, and rise of the very-long-period (VLP) seismic source towards the surface are interpreted as indicating an upward migration of the magma column in response to an increased magma input r…

geographyConduit processes; Effusive eruption; Geophysical monitoring; Stromboli volcano; Geochemistry and Petrologygeography.geographical_feature_categoryLateral eruptionVulcanian eruption010504 meteorology & atmospheric sciencesConduit processesStromboli volcanoMagma chamberConduit processe010502 geochemistry & geophysics01 natural sciencesGeophysical monitoringEffusive eruptionEffusive eruptionDense-rock equivalentVolcanoGeochemistry and PetrologyMagmaTephraGeologySeismology0105 earth and related environmental sciences
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